The significance of biotite selvedges in migmatites
- 1 January 1970
- journal article
- research article
- Published by Cambridge University Press (CUP) in Geological Magazine
- Vol. 107 (1), 21-24
- https://doi.org/10.1017/s0016756800054650
Abstract
Summary The biotite selvedges around potash-feldspar rich leucosome material in migmatites originate at phase boundaries between rocks containing hydrothermal and silicate pore-fluids and are thus indicative of incipient anatexis.Keywords
This publication has 9 references indexed in Scilit:
- On the solubility of albite in supercritical water in the range of 400 degrees to 600 degrees C and 750 to 3500 barsAmerican Journal of Science, 1968
- Plagioclase compositions and non-anatectic origin of migmatitic gneisses in Northern Cascade mountains of Washington StateContributions to Mineralogy and Petrology, 1968
- Genesis of migmatites from the palmer region of south AustraliaChemical Geology, 1966
- Experimental anatexis and genesis of migmatites: A replyContributions to Mineralogy and Petrology, 1966
- Major element composition of the Loch Coire migmatite complex, Sutherland, ScotlandContributions to Mineralogy and Petrology, 1966
- A chemical study of some rocks of the Moine Series of ScotlandQuarterly Journal of the Geological Society, 1965
- Alkali ion exchange between vapor and feldspar phasesAmerican Journal of Science, 1963
- The migmatitic Older Granodiorite of Thorr district, Co. DonegalQuarterly Journal of the Geological Society, 1952
- Phase relations at the pegmatitic stage, [Part] 3 of Transport and deposition of the non-sulphide vein mineralsEconomic Geology, 1948